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- W2111014124 abstract "The origins of cumulate rocks are re-examined in the light of new concepts in the fluid dynamics of crystallising systems. We propose that during the formation of adcumulate rocks, compositional convection allows continuous exchange of melt in the pores of a cumulus pile with the main magma reservoir. We consider this explanation to be physically more plausible than that proposed in the conventional cumulus theory. We present an experimental study of crystallisation in a porous medium to illustrate the process, and a theoretical analysis to demonstrate its applicability to magma chambers. We also consider factors which may inhibit convection and thus lead to the formation of meso- and orthocumulates. Finally we suggest how these ideas may be used to understand the distribution of these different rock types in layered intrusions." @default.
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- W2111014124 date "1984-01-01" @default.
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- W2111014124 title "The role of compositional convection in the formation of adcumulate rocks" @default.
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- W2111014124 doi "https://doi.org/10.1016/0024-4937(84)90014-8" @default.
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